Kohlschütter is a lunarimpact crater that cannot be viewed directly from the Earth as it lies on the Moon's far side. It is located a couple of hundred kilometers to the southeast of the Mare Moscoviense, and due south of the smaller crater Nagaoka. It is a relatively isolated formation surrounded by a multitude of smaller impacts typical of the battered far side.
The outer rim of Kohlschütter is worn and eroded, with a small crater across the northwest side, and smaller impacts along the west and northeastern edge. The southern rim is more shallow than elsewhere. The interior floor is relatively level, and unlike most far-side craters, it is filled with mare material.[1] Despite its small size, the mare has a short sinuous rille west of the central peak and a wrinkle ridge east of it.
^The geologic history of the Moon, 1987, Wilhelms, Don E.; with sections by McCauley, John F.; Trask, Newell J. USGS Professional Paper: 1348. (online), Figure 5-2
Menzel, D. H.; Minnaert, M.; Levin, B.; Dollfus, A.; Bell, B. (1971). "Report on Lunar Nomenclature by the Working Group of Commission 17 of the IAU". Space Science Reviews. 12 (2): 136–186. Bibcode:1971SSRv...12..136M. doi:10.1007/BF00171763. S2CID122125855.